Fig. 1: Variations of annual mean surface temperature, matching rates between simulations and observations, and sea ice depth in the Southern Hemisphere under 580–560 Ma continental configurations and various pCO2. | Nature Communications

Fig. 1: Variations of annual mean surface temperature, matching rates between simulations and observations, and sea ice depth in the Southern Hemisphere under 580–560 Ma continental configurations and various pCO2.

From: Maintenance of the great late Ediacaran ice age

Fig. 1: Variations of annual mean surface temperature, matching rates between simulations and observations, and sea ice depth in the Southern Hemisphere under 580–560 Ma continental configurations and various pCO2.The alt text for this image may have been generated using AI.

a Simulated annual mean surface temperature for pCO2 = 35 ppmv; (b) glacial matching rates between simulations and observations, in which the blue and orange dots represent the scenarios shown in Figure S1f–j and Figure S1k–o, respectively; (c) sea ice thickness in the Southern Hemisphere. Black values in panels are the pCO2 (ppmv) for the dots nearby.

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